REMOTE SENSING DETERMINATION OF BOUNDARIES IN ICE SHEETS FORMED BY GEOMAGNETIC FIELD REVERSALS

dc.contributor.authorYakupov V.S.
dc.contributor.authorYakupov M.V.
dc.contributor.authorYakupov S.V.
dc.date.accessioned2022-01-12T07:50:47Z
dc.date.available2022-01-12T07:50:47Z
dc.date.issued2003
dc.description.abstractConsidered is the possibility of remote, upon motion from the Earth as well as air, detecting, isolating and determining the bedding depth of boundaries in magnetization formed in polar glacier ice strata by geomagnetic field reversals, using correlating of results of radiolocation probing with magnetic and electric pulses. It enables to investigate the glacier development dynamics in time and space. The investigation depth is sufficient for studying the whole ice strata of any polar glaciers.
dc.identifierhttps://www.elibrary.ru/item.asp?id=13424475
dc.identifier.citationDoklady Earth Sciences, 2003, 393, 8, 1200-1203
dc.identifier.issn1028-334X
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/34225
dc.titleREMOTE SENSING DETERMINATION OF BOUNDARIES IN ICE SHEETS FORMED BY GEOMAGNETIC FIELD REVERSALS
dc.typeСтатья

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